Different origins of Cu-Pb-Zn-bearing and W-bearing granites

The Nanling Range of South China is world famous for its widely developed multiple-aged granitic magmatism and related polymetallic mineralization. Various kinds of granites have distinct diversities in terms of metallogenic specialization. A recent research revealed the different origins of the Middle-Late Jurassic Cu-Pb-Zn-bearing and W-bearing granites in the Nanling Range.

The related article is entitled "Petrogenetic differences between the Middle-Late Jurassic Cu-Pb-Zn-bearing and W-bearing granites in the Nanling Range, South China: A case study of the Tongshanling and Weijia deposits in southern Hunan Province", and was published in the Issue 7, Volume 60 (2017) of the Science China Earth Sciences as the cover paper authored by the research group led by Prof. LU JianJun of Nanjing University.

The Middle-Late Jurassic Cu-Pb-Zn-bearing and W-bearing granites in the Nanling Range are obviously different in terms of their petrography and geochemistry. However, the mechanism that created these differences has not been well understood. In general, the W-bearing granites are considered as to be the products of partial melting of an old metasedimentary basement, however, the petrogenesis of the Cu-Pb-Zn-bearing granites is still controversial. There is a time gap of about 5 Ma between the two different types of ore-bearing granites, the significance of which still requires further investigation.

Based on detailed geochronological and geochemical studies of both the Tongshanling Cu-Pb-Zn-bearing and Weijia W-bearing granites in southern Hunan Province and combined with the other Middle-Late Jurassic Cu-Pb-Zn-bearing and W-bearing granites in the Nanling Range, a genetic model of the two different types of ore-bearing granites has been proposed (Figure 1). Asthenosphere upwelling and basaltic magma underplating were induced by the subduction of the palaeo-Pacific plate. The underplated basaltic magmas provided heat to cause a partial melting of the mafic amphibolitic basement in the lower crust, resulting in the formation of granodioritic magmas related Cu-Pb-Zn mineralization. As the underplating of basaltic magmas developing, the muscovite-rich metasedimentary basement in the upper-middle crust was partially melted to generate W-bearing granitic magmas. The compositional difference of granite sources accounted for the metallogenic specialization, and the non-simultaneous partial melting of one source followed by the other brought about a time gap of about 5 Ma between the Cu-Pb-Zn-bearing and W-bearing granites.

This research provides a new viewpoint for understanding the metallogenic specialization of granites. It not only improves the knowledge of the metallogenesis of granites and enlightens prospecting and exploration in the Nanling Range, but also provides valuable reference for the study of granite-related metallogenesis in South China and even in the world.

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This research was funded by the National Natural Science Foundation of China (Grant No. 41273053), the National Key Basic Research Program of China (Grant No. 2012CB416702), and the Sino-French Cai Yuanpei Program of China Scholarship Council.

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